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dc.contributor.authorOrozco, Miguel
dc.date.accessioned2020-07-09T10:39:50Z
dc.date.available2020-07-09T10:39:50Z
dc.date.issued1986
dc.identifier.urihttp://hdl.handle.net/10272/18493
dc.description.abstractFrom microstructures and quartz c-axis fabric analysis the characterization of the «Mulhacen/Veleta ductil shear zone» is made. The existence of important eastward directed thrustings predating the S-N movements is inferred. These eastward thrustings must be taken into account in any tectonic reconstruction of the Betic-Riffean Orogenes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherThrustinges_ES
dc.subject.otherFabrices_ES
dc.subject.otherBetic orogenes_ES
dc.titleFábrica de cuarzo y cabalgamientos hacia el ENE en Sierra Nevada y Sierra de los Filabres (Cordilletas Béticas)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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